Geodiversity Issues

GEODIVERSITY AND QUARRYING


Coldstones Quarry
© Hanson

Aggregates are sand, gravel, and crushed rock used by the construction industry.

The Project Area is the key area in North Yorkshire for the production of aggregates. In 2003, the nine active quarries in the project area produced approximately 6 million (75%) of the 8 million tonnes of aggregate quarried in the County. Hanson plc, Lafarge and Tarmac Ltd operate the nine quarries. All of the aggregate produced is from crushed rock either greywacke or limestone.

Seven of the quarries are located in the southern part of the Yorkshire Dales National Park and one is located in the Nidderdale Area of Outstanding Natural Beauty. Quarrying in such landscape sensitive areas is seen by some groups as highly controversial but the quarries are, however, important to both the national and local economies. This issue requires very careful management.

In the Project Area, six of the geological SSSIs, for example Greenhow Quarry and Hambleton Quarry, are former aggregate quarries, and provide evidence of how mineral working can increase geodiversity by exposing previously unseen rock exposures and geological structures.

ACTIVE QUARRIES IN THE PROJECT AREA
QUARRY GRID
REFERENCE
AUTHORITY COMPANY AGGREGATE
Arcow 3803 4704 YDNP Tarmac greywacke
Coldstones 4125 4642 Harrogate / Nidderdale AONB Hanson Carboniferous limestone
Dry Rigg 3804 4694 YDNP Lafarge greywacke
Giggleswick 3810 4650 YDNP Hanson Carboniferous limestone
Horton 3800 4721 YDNP Hanson Carboniferous limestone
Ingleton 3705 4742 YDNP Hanson greywacke
Skipton Rock 4014 4532 Craven Tarmac Carboniferous limestone
Swinden 3983 4615 YDNP Tarmac Carboniferous limestone
Threshfield 3977 4645 YDNP Tarmac Carboniferous limestone

GEODIVERSITY AND ARCHAEOLOGY


Sharrow Hill Lime Quarry
© YDNPA

The geology and geological resources of the area have been used by people who have settled in the area since the end of the last ice age. The landscapes we are so proud of today result from the interaction of this exploitation, the geology, climate and time.

The earliest known evidence of human activity in the area has been found in caves in the Yorkshire Dales National Park and is dated to approximately 12,300 BC.

Many archaeological sites in the area are recognised as being nationally important and have been protected by being designated as Scheduled Ancient Monuments. A large number of them are also important for their geodiversity. This is particularly true of sites such as Moulds Side in Arkengarthdale, which includes the very impressive Stodart and Hungry Hushes, Dam Rigg Lead Mine and numerous levels, and the complex of lead mine workings on Grassington Moor.

For more information go to: www.outofoblivion.org.uk
NOTE: NYGP is not reponsible for the content of external sites


Hard Level Gill showing evidence of former mining activity
© R. White YDNPA

 

 

 

 

GEODIVERSITY AND BIODIVERSITY

The rock type of an area is one of the major abiotic factors which determines biodiversity, through its weathering to form soil and its control on the movement of water. Specific habitats with their distinctive plant communities can be related to variations in the surface geology.

Many of the habitats in the area are Priority habitats in the UK Biodiversity Action Plan (UK BAP) and specific habitat action plans have been prepared for them in 'Nature in the Dales – A Biodiversity Action Plan for the Yorkshire Dales National Park ' (2000) and where appropriate in the Local BAPs published or in preparation - Harrogate District BAP, Richmondshire BAP and Craven BAP (outside the YDNP), developed in partnerships led by North Yorkshire County Council and the district councils.


More information:
www.ukbap.org.uk
www.yorkshiredales.org.uk
NOTE: NYGP is not reponsible for the content of external sites

HABITAT TYPES
Key habitat UK BAP Nature in the Dales Harrogate District BAP Richmond-shire BAP Craven BAP
Ancient and/or species-rich hedgerows

Blanket bog

Caves and natural rock exposures

 
 
 
Cereal field margins (and arable)

Eutrophic standing waters

Fens

Floodplain grazing marsh

 

Gardens    

Limestone pavements

     
Lowland calcareous grassland

Lowland meadows

 

Lowland raised bog

   

Lowland wood pasture and parkland

Mesotrophic lakes

 

 
Moorland edge    

 
Other standing waters

   
Other woodland  

     
Purple moor grass and rush pasture.

     
Reedbeds

 

 
Rivers and streams  

Rock outcrops, scars, scree and spoil  

     
Scrub  

Species-rich road and rail verges  

Upland calcareous grassland

Upland hay meadows

 

Upland heathland

Upland mixed ashwoods

 

Upland oakwood

Wet acidic grassland

   

Wet woodland

HABITAT TYPES RELATED TO SURFACE GEOLOGY

Underlying geology

Key habitat

UK BAP

Nature in the Dales

Harrogate District BAP

Richmondshire BAP

Craven BAP

Carboniferous Limestone

Caves and natural rock exposures

     

Fens

Limestone pavements

     

Limestone quarries

 

     

Lowland calcareous grassland

Mines

 

     

Mine spoil

 

     

Rock outcrops, scars, scree and spoil

 

     

Upland calcareous grassland

Upland mixed ashwoods

 

Millstone Grit

Blanket bog

Fens

Gritstone and shale quarries

 

     

Lowland raised bog

   

Mines

 

     

Mine spoil

 

     

Rock outcrops, scars, scree and spoil

 

     

Upland heathland

Upland oakwood

Wet acidic grassland

   

Alluvial and glacial deposits

Ancient and/or species-rich hedgerows

Cereal field margins (and arable)

Fens

Floodplain grazing marsh

 

Lowland wood pasture and parkland

Reedbeds

 

 

Species-rich road and rail verges

 

Upland hay meadows

 

Wet woodland

 

 

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